supported by the National Natural Science Foundation of China(No.42172064)。
Subduction initiation and termination represent the birth and death of a subduction zone and are inevitable elements of terrestrial plate tectonics.Increasing evidence demonstrates that subduction zone processes did n...
the National Natural Science Foundation of China(Grant Nos.91955206,41603038);Second Tibetan Plateau Scientific Expedition and Research program(Grant No.2019QZKK0803);Scientific Research Foundation for Advanced Scholars;West Yunnan University of Applied Sciences(Grant No.2022RCKY0004);Yunnan Fundamental Research Projects(Grant No.202301AT070012).
In this study,zircon U-Pb dating of volcanic rocks from the Zhongba ophiolite of the Yarlung Zangbo Suture Zone(YZSZ)in southern Xizang(Tibet)yielded an age of 247±3 Ma.According to whole rock geochemical and Sr-NdPb...
The research paper"Geodynamic processes of the southeastern Neo-Tethys Ocean and the formation mechanism of the curved subduction system in Southeast Asia"(Sci China Earth Sci,2023,66:703-717)contained errors.The corr...
supported financially by the Vice Chancellor for Research and Technology at University of Isfahan。
Precise taxonomy and the chronostratigraphic calibration of the Middle Eocene Alveolina from Central Iran is here undertaken from the Chah-Talkh section of the southern Sabzevar region(Central Iran). We have identifie...
supported by the National Natural Science Foundation of China (Grant Nos.42025201,92155001,41802062,41888101);the Second Tibetan Plateau Scientific Expedition and Research Program (Grant No.2019QZKK0801)。
The evolution and final closure of the Neo-Tethys Ocean are one of the most important geological events that have occurred on Earth since the Mesozoic.However,the evolution of the Neo-Tethys is not well constrained,in...
supported by the National Natural Science Foundation of China(Grant Nos.42025601,41890811&92155203)。
Southeast Asia is located at the intersection of the Tethys and Pacific domains. The superimposed effects of the two tectonic domains have resulted in complicated deep structure, surface magma responses, and dynamic p...
The authors extend their appreciation to Researchers Supporting Project (No. RSP2023R139)。
The Toarcian Marrat Formation is exposed in outcrops in central Saudi Arabia and displays a variety of clastic and carbonate facies associated with well-preserved depositional geometries. It is unconformably overlies ...
Imam Khomeini International University for all its support。
This study investigates the Gurpi Formation in the northeast of Izeh,southwestern Iran.In this study,59 species and 34 genera were determined.Biostratigraphy allows the identification of zones CC21 to CC26,which is eq...
End-Permian Gondwana siliciclastics (50 - 70 m) of the Um Irna F exposed along the NE Dead Sea, exhibit carbonate-free fining upward cycles (FUC) deposited during acid flash flood events under tropical climate. Severa...
supported by the National Natural Science Foundation of China(Grant No.41688103);the International Cooperation Program of the Chinese Academy of Sciences(Grant No.GJHZ1776)。
The Neo-Tethys Ocean was an eastward-gaping triangular oceanic embayment between Laurasia to the north and Gondwana to the south.The Neo-Tethys Ocean was initiated from the Early Permian with mircoblocks rifted from t...